1974
DOI: 10.1016/0148-9062(74)91120-6
|View full text |Cite
|
Sign up to set email alerts
|

Investigations of the relations among residual strain, fabric, fracture and ultrasonic attenuation and velocity in rocks

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
1
1

Citation Types

0
2
0

Year Published

1979
1979
2020
2020

Publication Types

Select...
3
1

Relationship

0
4

Authors

Journals

citations
Cited by 4 publications
(2 citation statements)
references
References 0 publications
0
2
0
Order By: Relevance
“…11). The compressional wave velocity is slowest perpendicular to a microcrack alignment (Friedman and Bur 1974) provided that the compression applied to the specimen during measurement is not large enough to close the microcracks. The curves plotted for velocity against compression (Fig.…”
Section: Laboratory Tests On Sandstonesmentioning
confidence: 99%
“…11). The compressional wave velocity is slowest perpendicular to a microcrack alignment (Friedman and Bur 1974) provided that the compression applied to the specimen during measurement is not large enough to close the microcracks. The curves plotted for velocity against compression (Fig.…”
Section: Laboratory Tests On Sandstonesmentioning
confidence: 99%
“…If, however, we assume that most of the spread in the errors is caused by small-scale topography and accept the mean values, then anisotropy on the order of 0.2 km/s may exist. Since the velocity gradients at the site indicate that the cracks on all scales are almost completely closed at the bottom of Layer 2, the anisotropy could be related to crystal orientation or residual fabric (Christensėn, 1972;Friedman and Bur, 1974).…”
Section: Anisotropymentioning
confidence: 99%